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TRANSIENT LUNAR PHENOMENA: REGULARITY and REALITY Arlin P
The Astrophysical Journal, 697:1–15, 2009 May 20 doi:10.1088/0004-637X/697/1/1 C 2009. The American Astronomical Society. All rights reserved. Printed in the U.S.A. TRANSIENT LUNAR PHENOMENA: REGULARITY AND REALITY Arlin P. S. Crotts Department of Astronomy, Columbia University, Columbia Astrophysics Laboratory, 550 West 120th Street, New York, NY 10027, USA Received 2007 June 27; accepted 2009 February 20; published 2009 April 30 ABSTRACT Transient lunar phenomena (TLPs) have been reported for centuries, but their nature is largely unsettled, and even their existence as a coherent phenomenon is controversial. Nonetheless, TLP data show regularities in the observations; a key question is whether this structure is imposed by processes tied to the lunar surface, or by terrestrial atmospheric or human observer effects. I interrogate an extensive catalog of TLPs to gauge how human factors determine the distribution of TLP reports. The sample is grouped according to variables which should produce differing results if determining factors involve humans, and not reflecting phenomena tied to the lunar surface. Features dependent on human factors can then be excluded. Regardless of how the sample is split, the results are similar: ∼50% of reports originate from near Aristarchus, ∼16% from Plato, ∼6% from recent, major impacts (Copernicus, Kepler, Tycho, and Aristarchus), plus several at Grimaldi. Mare Crisium produces a robust signal in some cases (however, Crisium is too large for a “feature” as defined). TLP count consistency for these features indicates that ∼80% of these may be real. Some commonly reported sites disappear from the robust averages, including Alphonsus, Ross D, and Gassendi. -
50. Obletnica Pristanka Na Luni in Pomen Osvajanja Vesolja Za Geodezijo 50Th Anniversary of the Moon Landing and the Importance
GEODETSKI VESTNIK | 63/4 | 50. OBLETNICA PRISTANKA 50TH ANNIVERSARY OF NA LUNI IN POMEN THE MOON LANDING AND OSVAJANJA VESOLJA ZA THE IMPORTANCE OF GEODEZIJO CONQUERING SPACE FOR GEODESY Sandi Berk STROKOVNE RAZPRAVE | PROFESSIONAL DISCUSSIONS RAZPRAVE STROKOVNE 1 UVOD Letos mineva petdeset let od prvega obiska človeka na edini Zemljini luni – Mesecu (v nadaljevanju kar: Luna). Ta »majhen korak za človeka, a velikanski skok za človeštvo« je bil storjen 20. julija 1969, ko sta Neil Armstrong in Edwin Aldrin v lunarnem modulu Eagle (tj. Orel) pristala poleg Malega zahodnega kraterja v Morju tišine (slika 1). Okrogla obletnica je priložnost, da se ozremo nazaj in osvežimo dogod- ke iz pionirskih časov osvajanja vesolja. Hkrati lahko osvetlimo pomen takratnih podvigov ter njihove učinke na tehnološki razvoj in tudi napredek geodezije. Slika 1: Armstrongova fotografija Aldrina ob nameščenem seizmografu; nad njim je reflektor za lasersko merjenje oddaljenosti od Zemlje, desno zgoraj pa je lunarni modul Eagle (vir: NASA, 2019). | 589 | | 63/4 | GEODETSKI VESTNIK Kje se sploh prične vesolje – kako visoko je treba poleteti? Mejo med Zemljino atmosfero in vesoljskim prostorom (angl. outer space) imenujemo Kármánova ločnica in je približno sto kilometrov nad površjem Zemlje. Nad to višino za letenje ne veljajo več zakoni aerodinamike, ampak je mogoče zgolj še letenje po zakonih balistike, torej na raketni pogon. Pomembna je tudi v pravnem smislu, saj se tu konča zračni prostor držav in začne veljati mednarodno vesoljsko pravo. Kot vemo, letijo potniška letala na višini približno deset kilometrov. Nedavni rekordni polet z jadralnim letalom je dosegel višino 23 kilometrov nad morjem, vendar s pomočjo stratosferskih zavetrnih valov, ki nastajajo zaradi izredno močnih zračnih tokov med visokimi gorskimi vrhovi Andov (Ebbesen Jensen, 2019). -
The Soviet Space Program
C05500088 TOP eEGRET iuf 3EEA~ NIE 11-1-71 THE SOVIET SPACE PROGRAM Declassified Under Authority of the lnteragency Security Classification Appeals Panel, E.O. 13526, sec. 5.3(b)(3) ISCAP Appeal No. 2011 -003, document 2 Declassification date: November 23, 2020 ifOP GEEAE:r C05500088 1'9P SloGRET CONTENTS Page THE PROBLEM ... 1 SUMMARY OF KEY JUDGMENTS l DISCUSSION 5 I. SOV.IET SPACE ACTIVITY DURING TfIE PAST TWO YEARS . 5 II. POLITICAL AND ECONOMIC FACTORS AFFECTING FUTURE PROSPECTS . 6 A. General ............................................. 6 B. Organization and Management . ............... 6 C. Economics .. .. .. .. .. .. .. .. .. .. .. ...... .. 8 III. SCIENTIFIC AND TECHNICAL FACTORS ... 9 A. General .. .. .. .. .. 9 B. Launch Vehicles . 9 C. High-Energy Propellants .. .. .. .. .. .. .. .. .. 11 D. Manned Spacecraft . 12 E. Life Support Systems . .. .. .. .. .. .. .. .. 15 F. Non-Nuclear Power Sources for Spacecraft . 16 G. Nuclear Power and Propulsion ..... 16 Te>P M:EW TCS 2032-71 IOP SECl<ET" C05500088 TOP SECRGJ:. IOP SECREI Page H. Communications Systems for Space Operations . 16 I. Command and Control for Space Operations . 17 IV. FUTURE PROSPECTS ....................................... 18 A. General ............... ... ···•· ................. ····· ... 18 B. Manned Space Station . 19 C. Planetary Exploration . ........ 19 D. Unmanned Lunar Exploration ..... 21 E. Manned Lunar Landfog ... 21 F. Applied Satellites ......... 22 G. Scientific Satellites ........................................ 24 V. INTERNATIONAL SPACE COOPERATION ............. 24 A. USSR-European Nations .................................... 24 B. USSR-United States 25 ANNEX A. SOVIET SPACE ACTIVITY ANNEX B. SOVIET SPACE LAUNCH VEHICLES ANNEX C. SOVIET CHRONOLOGICAL SPACE LOG FOR THE PERIOD 24 June 1969 Through 27 June 1971 TCS 2032-71 IOP SLClt~ 70P SECRE1- C05500088 TOP SEGR:R THE SOVIET SPACE PROGRAM THE PROBLEM To estimate Soviet capabilities and probable accomplishments in space over the next 5 to 10 years.' SUMMARY OF KEY JUDGMENTS A. -
Spacecraft Deliberately Crashed on the Lunar Surface
A Summary of Human History on the Moon Only One of These Footprints is Protected The narrative of human history on the Moon represents the dawn of our evolution into a spacefaring species. The landing sites - hard, soft and crewed - are the ultimate example of universal human heritage; a true memorial to human ingenuity and accomplishment. They mark humankind’s greatest technological achievements, and they are the first archaeological sites with human activity that are not on Earth. We believe our cultural heritage in outer space, including our first Moonprints, deserves to be protected the same way we protect our first bipedal footsteps in Laetoli, Tanzania. Credit: John Reader/Science Photo Library Luna 2 is the first human-made object to impact our Moon. 2 September 1959: First Human Object Impacts the Moon On 12 September 1959, a rocket launched from Earth carrying a 390 kg spacecraft headed to the Moon. Luna 2 flew through space for more than 30 hours before releasing a bright orange cloud of sodium gas which both allowed scientists to track the spacecraft and provided data on the behavior of gas in space. On 14 September 1959, Luna 2 crash-landed on the Moon, as did part of the rocket that carried the spacecraft there. These were the first items humans placed on an extraterrestrial surface. Ever. Luna 2 carried a sphere, like the one pictured here, covered with medallions stamped with the emblem of the Soviet Union and the year. When Luna 2 impacted the Moon, the sphere was ejected and the medallions were scattered across the lunar Credit: Patrick Pelletier surface where they remain, undisturbed, to this day. -
Water on the Moon, III. Volatiles & Activity
Water on The Moon, III. Volatiles & Activity Arlin Crotts (Columbia University) For centuries some scientists have argued that there is activity on the Moon (or water, as recounted in Parts I & II), while others have thought the Moon is simply a dead, inactive world. [1] The question comes in several forms: is there a detectable atmosphere? Does the surface of the Moon change? What causes interior seismic activity? From a more modern viewpoint, we now know that as much carbon monoxide as water was excavated during the LCROSS impact, as detailed in Part I, and a comparable amount of other volatiles were found. At one time the Moon outgassed prodigious amounts of water and hydrogen in volcanic fire fountains, but released similar amounts of volatile sulfur (or SO2), and presumably large amounts of carbon dioxide or monoxide, if theory is to be believed. So water on the Moon is associated with other gases. Astronomers have agreed for centuries that there is no firm evidence for “weather” on the Moon visible from Earth, and little evidence of thick atmosphere. [2] How would one detect the Moon’s atmosphere from Earth? An obvious means is atmospheric refraction. As you watch the Sun set, its image is displaced by Earth’s atmospheric refraction at the horizon from the position it would have if there were no atmosphere, by roughly 0.6 degree (a bit more than the Sun’s angular diameter). On the Moon, any atmosphere would cause an analogous effect for a star passing behind the Moon during an occultation (multiplied by two since the light travels both into and out of the lunar atmosphere). -
Apollo Over the Moon: a View from Orbit (Nasa Sp-362)
chl APOLLO OVER THE MOON: A VIEW FROM ORBIT (NASA SP-362) Chapter 1 - Introduction Harold Masursky, Farouk El-Baz, Frederick J. Doyle, and Leon J. Kosofsky [For a high resolution picture- click here] Objectives [1] Photography of the lunar surface was considered an important goal of the Apollo program by the National Aeronautics and Space Administration. The important objectives of Apollo photography were (1) to gather data pertaining to the topography and specific landmarks along the approach paths to the early Apollo landing sites; (2) to obtain high-resolution photographs of the landing sites and surrounding areas to plan lunar surface exploration, and to provide a basis for extrapolating the concentrated observations at the landing sites to nearby areas; and (3) to obtain photographs suitable for regional studies of the lunar geologic environment and the processes that act upon it. Through study of the photographs and all other arrays of information gathered by the Apollo and earlier lunar programs, we may develop an understanding of the evolution of the lunar crust. In this introductory chapter we describe how the Apollo photographic systems were selected and used; how the photographic mission plans were formulated and conducted; how part of the great mass of data is being analyzed and published; and, finally, we describe some of the scientific results. Historically most lunar atlases have used photointerpretive techniques to discuss the possible origins of the Moon's crust and its surface features. The ideas presented in this volume also rely on photointerpretation. However, many ideas are substantiated or expanded by information obtained from the huge arrays of supporting data gathered by Earth-based and orbital sensors, from experiments deployed on the lunar surface, and from studies made of the returned samples. -
Mapping and GIS-Analyses of the Lunokhod-1 Landing Site
43rd Lunar and Planetary Science Conference (2012) 1750.pdf Mapping and GIS-Analyses of the Lunokhod-1 Landing Site. E. Gusakova1, I. Karachevtseva1, K.Shingareva1, J. Oberst1,2,3, O. Peters2, M.Wählisch2, and M. S. Robinson4. 1Moscow State University of Geodesy and Cartography (MIIGAiK), Gorokhovskiy per., 4, 105064, Moscow, Russia; 2German Aerospace Center (DLR); 3 Technical Uni- versity of Berlin, Germany; 4Arizona State University, USA Introduction: The Soviet spacecraft Luna 17 was small craters, which could be compare with results of launched towards the Moon in November 1970 and mapping that had been carried out during the Lunok- deployed Lunokhod-1, the first rover to explore an hod-1 mission. We conclude that LRO NAC images extraterrestrial surface. Until October 1971, Lunokhod- can be used for cartography support at high level of 1 acquired about 20,000 TV pictures and 206 stereo detail for characterization of future landing sites such images along its traverse [1]. Using recent new high as LUNA-GLOB and LUNA-RESOURCE. resolution images we mapped the landing site and tra- Reference: [1] Barsukov V.L. et. al. (1978) Pe- verse route, using automated GIS-oriented mapping. redvijnaya laboratoriya na Lune Lunokhod-1, Vol. 2. Sources: We used high resolution Digital Eleva- Nauka (in Russian). [2] Oberst J. et al. (2010) LPSC tion Model (DEM) and orthoimage from photogram- XLI, Abstract #2051. [3] Kneissl T. et al. (2011) Pla- metric processing of Lunar Reconnaissance Orbiter net. Space Sci., 59, 1243-1254. [4] Karachevtseva I. et Camera (LROC) Narrow Angle Camera (NAC) stereo al. (2011) The Book of Abstracts of the 2-nd Moscow images [2] with a spatial resolution of 0.5 m/pixel Solar System Symposium (2M-S3), Space Research (M150749234, M150756018). -
Deep Space Chronicle Deep Space Chronicle: a Chronology of Deep Space and Planetary Probes, 1958–2000 | Asifa
dsc_cover (Converted)-1 8/6/02 10:33 AM Page 1 Deep Space Chronicle Deep Space Chronicle: A Chronology ofDeep Space and Planetary Probes, 1958–2000 |Asif A.Siddiqi National Aeronautics and Space Administration NASA SP-2002-4524 A Chronology of Deep Space and Planetary Probes 1958–2000 Asif A. Siddiqi NASA SP-2002-4524 Monographs in Aerospace History Number 24 dsc_cover (Converted)-1 8/6/02 10:33 AM Page 2 Cover photo: A montage of planetary images taken by Mariner 10, the Mars Global Surveyor Orbiter, Voyager 1, and Voyager 2, all managed by the Jet Propulsion Laboratory in Pasadena, California. Included (from top to bottom) are images of Mercury, Venus, Earth (and Moon), Mars, Jupiter, Saturn, Uranus, and Neptune. The inner planets (Mercury, Venus, Earth and its Moon, and Mars) and the outer planets (Jupiter, Saturn, Uranus, and Neptune) are roughly to scale to each other. NASA SP-2002-4524 Deep Space Chronicle A Chronology of Deep Space and Planetary Probes 1958–2000 ASIF A. SIDDIQI Monographs in Aerospace History Number 24 June 2002 National Aeronautics and Space Administration Office of External Relations NASA History Office Washington, DC 20546-0001 Library of Congress Cataloging-in-Publication Data Siddiqi, Asif A., 1966 Deep space chronicle: a chronology of deep space and planetary probes, 1958-2000 / by Asif A. Siddiqi. p.cm. – (Monographs in aerospace history; no. 24) (NASA SP; 2002-4524) Includes bibliographical references and index. 1. Space flight—History—20th century. I. Title. II. Series. III. NASA SP; 4524 TL 790.S53 2002 629.4’1’0904—dc21 2001044012 Table of Contents Foreword by Roger D. -
Planetary Rover Mobility on Loose Soil
PLANETARYROVERMOBILITYONLOOSESOIL: TERRAMECHANICSTHEORYFORSIDESLIPPREDICTION ANDCOMPENSATION nicolò carletti Supervisor: Prof. Michéle Lavagna Master of Science Space Engineering Department of Aerospace Science and Technology Politecnico di Milano December 2016 – 816663 ABSTRACT The aim of this thesis is to develop a model which can predict a mobile trajectory profile of the rover under loose soil condition. The study also encapsulates a traversal run in a sloped terrain without the skid characteristics. The geometry and features are defined to model the rover as known as Moonraker: the lunar rover of the team HAKUTO, competing for the Google Lunar XPRIZE. After a brief introduction of the working environment, a chapter is de- dicated to the modeling of the forces generated from the interaction between wheels with soil, depending on the slip ratio and the slip angle. The used model is the one proposed by G. Ishigami [6, 7, 8, 9], based on the work of M. G. Bekker [1, 2] and J. Y. Wong [3] and modi- fied, according to what proposed by M. Sutoh [11, 12, 13], to explicitly consider the grouser effect. The model is verified through One-Wheel tests. The equations of motion are retrieved and the numerical simulation with iterative loop is described. The desired state is reached imposing arbitrary inputs to the wheels. Two input strategies are discussed: torque input and velocity input. The resulting motion is compared with tests on both controlled (sand- box) and uncontrolled environment. The former is mainly used to ve- rify the precision of the model, and the latter to prove the sensibility to the ground properties. -
The Development of Wheels for the Lunar Roving Vehicle
NASA/TM—2009-215798 The Development of Wheels for the Lunar Roving Vehicle Vivake Asnani, Damon Delap, and Colin Creager Glenn Research Center, Cleveland, Ohio December 2009 NASA STI Program . in Profi le Since its founding, NASA has been dedicated to the • CONFERENCE PUBLICATION. Collected advancement of aeronautics and space science. The papers from scientifi c and technical NASA Scientifi c and Technical Information (STI) conferences, symposia, seminars, or other program plays a key part in helping NASA maintain meetings sponsored or cosponsored by NASA. this important role. • SPECIAL PUBLICATION. Scientifi c, The NASA STI Program operates under the auspices technical, or historical information from of the Agency Chief Information Offi cer. It collects, NASA programs, projects, and missions, often organizes, provides for archiving, and disseminates concerned with subjects having substantial NASA’s STI. The NASA STI program provides access public interest. to the NASA Aeronautics and Space Database and its public interface, the NASA Technical Reports • TECHNICAL TRANSLATION. English- Server, thus providing one of the largest collections language translations of foreign scientifi c and of aeronautical and space science STI in the world. technical material pertinent to NASA’s mission. Results are published in both non-NASA channels and by NASA in the NASA STI Report Series, which Specialized services also include creating custom includes the following report types: thesauri, building customized databases, organizing and publishing research results. • TECHNICAL PUBLICATION. Reports of completed research or a major signifi cant phase For more information about the NASA STI of research that present the results of NASA program, see the following: programs and include extensive data or theoretical analysis. -
ILWS Report 137 Moon
Returning to the Moon Heritage issues raised by the Google Lunar X Prize Dirk HR Spennemann Guy Murphy Returning to the Moon Heritage issues raised by the Google Lunar X Prize Dirk HR Spennemann Guy Murphy Albury February 2020 © 2011, revised 2020. All rights reserved by the authors. The contents of this publication are copyright in all countries subscribing to the Berne Convention. No parts of this report may be reproduced in any form or by any means, electronic or mechanical, in existence or to be invented, including photocopying, recording or by any information storage and retrieval system, without the written permission of the authors, except where permitted by law. Preferred citation of this Report Spennemann, Dirk HR & Murphy, Guy (2020). Returning to the Moon. Heritage issues raised by the Google Lunar X Prize. Institute for Land, Water and Society Report nº 137. Albury, NSW: Institute for Land, Water and Society, Charles Sturt University. iv, 35 pp ISBN 978-1-86-467370-8 Disclaimer The views expressed in this report are solely the authors’ and do not necessarily reflect the views of Charles Sturt University. Contact Associate Professor Dirk HR Spennemann, MA, PhD, MICOMOS, APF Institute for Land, Water and Society, Charles Sturt University, PO Box 789, Albury NSW 2640, Australia. email: [email protected] Spennemann & Murphy (2020) Returning to the Moon: Heritage Issues Raised by the Google Lunar X Prize Page ii CONTENTS EXECUTIVE SUMMARY 1 1. INTRODUCTION 2 2. HUMAN ARTEFACTS ON THE MOON 3 What Have These Missions Left BehinD? 4 Impactor Missions 10 Lander Missions 11 Rover Missions 11 Sample Return Missions 11 Human Missions 11 The Lunar Environment & ImpLications for Artefact Preservation 13 Decay caused by ascent module 15 Decay by solar radiation 15 Human Interference 16 3. -
What's Hot on the Moon Tonight?: the Ultimate Guide to Lunar Observing
What’s Hot on the Moon Tonight: The Ultimate Guide to Lunar Observing Copyright © 2015 Andrew Planck All rights reserved. No part of this book may be reproduced in any written, electronic, recording, or photocopying without written permission of the publisher or author. The exception would be in the case of brief quotations embodied in the critical articles or reviews and pages where permission is specifically granted by the publisher or author. Although every precaution has been taken to verify the accuracy of the information contained herein, the publisher and author assume no responsibility for any errors or omissions. No liability is assumed for damages that may result from the use of information contained within. Books may be purchased by contacting the publisher or author through the website below: AndrewPlanck.com Cover and Interior Design: Nick Zelinger (NZ Graphics) Publisher: MoonScape Publishing, LLC Editor: John Maling (Editing By John) Manuscript Consultant: Judith Briles (The Book Shepherd) ISBN: 978-0-9908769-0-8 Library of Congress Catalog Number: 2014918951 1) Science 2) Astronomy 3) Moon Dedicated to my wife, Susan and to my two daughters, Sarah and Stefanie Contents Foreword Acknowledgments How to Use this Guide Map of Major Seas Nightly Guide to Lunar Features DAYS 1 & 2 (T=79°-68° E) DAY 3 (T=59° E) Day 4 (T=45° E) Day 5 (T=24° E.) Day 6 (T=10° E) Day 7 (T=0°) Day 8 (T=12° W) Day 9 (T=21° W) Day 10 (T= 28° W) Day 11 (T=39° W) Day 12 (T=54° W) Day 13 (T=67° W) Day 14 (T=81° W) Day 15 and beyond Day 16 (T=72°) Day 17 (T=60°) FINAL THOUGHTS GLOSSARY Appendix A: Historical Notes Appendix B: Pronunciation Guide About the Author Foreword Andrew Planck first came to my attention when he submitted to Lunar Photo of the Day an image of the lunar crater Pitatus and a photo of a pie he had made.